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AMIRA Project P544: Proterozoic sediment-hosted copper deposits. Quarterly progress reports and final report for the period July 2000 to October 2003.
The original objectives of this project were: 1) To understand the processes responsible for transporting, concentrating and fixing copper and other ore constituents during sedimentary basin evolution 2) To document the various stages and paragenesis...-
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Geochemical mapping of a copper mineral system, Lyndhurst area (for the ARC North Project). Final report, Project ADI RD01-126 [part of Accelerated Discovery Initiative Round 1, 2021].
As a part of searching for economic deposits of sediment-hosted copper (SHC) mineralisation that might have formed within rocks of the Adelaide Rift Complex Neoproterozoic sedimentation sequence occupying an area located due east of Lyndhurst in the...-
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RB 2012/00004 MARREE, South Australia, [geological map] sheet SH54-5. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The MARREE mapsheet area includes the south-western portion of the Strzelecki Desert plus parts of the Tirari Desert, north-western Flinders Ranges and north-eastern Willouran Ranges, between latitudes 29 to 30 degrees S and longitudes 138 to 139...-
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Published: 01 Apr 2012
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Eurelia - Carrieton area. Progress and final reports to licence expiry/full surrender for the period 1/11/1976 to 31/10/1977.
Exploration near Carrieton for possible economic stratiform copper deposits hosted by metasediments at the base of the Adelaidean System, as the culmination to a 9-year long programme carried over from Utah's former EL 137 and six prior tenements...-
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ExpNotes MARREE: Explanatory Notes MARREE
A new generation, second edition MARREE 1:250 000 scale geological map and its explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's latest geological mapping program (1993 to...-
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ExpNotes PARACHILNA (v2): Explanatory Notes PARACHILNA (second edition, 1999)
The PARACHILNA map area (31 to 32°S, 138 to 139.5°E) occupies the central Flinders Ranges which are made up of folded, mostly marine sedimentary Neoproterozoic and Cambrian rocks of the Adelaide Geosyncline, and adjoining plains underlain by Cainozoic...-
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